[HTML][HTML] The Northern Calcareous Alps revisited: Formation of a hyperextended margin and mantle exhumation in the Northern Calcareous Alps sector of the Neo …
Abstract The Neo-Tethys margin evolution is preserved in the Northern Calcareous Alps
(Eastern Alps), from Late Permian crustal stretching to Late Triassic oceanization. The …
(Eastern Alps), from Late Permian crustal stretching to Late Triassic oceanization. The …
Denudation history and palaeogeography of the Pyrenees and their peripheral basins: an 84-million-year geomorphological perspective
This review provides a synthesis of the evolution of the Pyrenees since~ 84 Ma and is
uniquely focused on analysing jointly and comparatively its peripheral pro-foreland, retro …
uniquely focused on analysing jointly and comparatively its peripheral pro-foreland, retro …
Evolution of the Alpine orogenic belts in the Western Mediterranean region as resolved by the kinematics of the Europe-Africa diffuse plate boundary
Abstract The West European collisional Alpine belts are the result of the inversion, initiated
in the middle Cretaceous, of the complex western Neotethys and the Atlantic continental rift …
in the middle Cretaceous, of the complex western Neotethys and the Atlantic continental rift …
[HTML][HTML] A reconstruction of Iberia accounting for Western Tethys–North Atlantic kinematics since the late-Permian–Triassic
The western European kinematic evolution results from the opening of the western
Neotethys and the Atlantic oceans since the late Paleozoic and the Mesozoic. Geological …
Neotethys and the Atlantic oceans since the late Paleozoic and the Mesozoic. Geological …
The Mesozoic Iberia-Eurasia diffuse plate boundary: A wide domain of distributed transtensional deformation progressively focusing along the North Pyrenean Zone
Plate kinematic reconstructions available for the Late Jurassic-Early Cretaceous eastward
drift and counterclockwise rotation of the Iberian plate imply a major left-lateral motion of …
drift and counterclockwise rotation of the Iberian plate imply a major left-lateral motion of …
Geodynamic evolution of a wide plate boundary in the Western Mediterranean, near-field versus far-field interactions
The present-day tectonic setting of the Western Mediterranean region, from the Pyrénées to
the Betics and from the Alps to the Atlas, results from a complex 3-D geodynamic evolution …
the Betics and from the Alps to the Atlas, results from a complex 3-D geodynamic evolution …
Role of rift-inheritance and segmentation for orogenic evolution: example from the Pyrenean-Cantabrian system
R Lescoutre, G Manatschal - Bulletin de la Société …, 2020 - pubs.geoscienceworld.org
The Basque-Cantabrian junction corresponds to an inverted rift accommodation zone at the
limit between the former hyperextended Pyrenean and Cantabrian rift segments. The …
limit between the former hyperextended Pyrenean and Cantabrian rift segments. The …
Crustal-scale balanced cross-section and restorations of the Central Pyrenean belt (Nestes-Cinca transect): Highlighting the structural control of Variscan belt and …
In this paper, we combined new field geological, structural, paleo-temperature and
subsurface data together with deep geophysical data to build a new 210 km-long crustal …
subsurface data together with deep geophysical data to build a new 210 km-long crustal …
The Nappe des Marbres unit of the Basque‐Cantabrian Basin: The tectono‐thermal evolution of a fossil hyperextended rift basin
The architecture of the Pyrenean‐Cantabrian belt results from the inversion of a series of
former Cretaceous rift basins. A HT‐LP metamorphic event dated at 105 to 85 Ma ago is …
former Cretaceous rift basins. A HT‐LP metamorphic event dated at 105 to 85 Ma ago is …
Fast dismantling of a mountain belt by mantle flow: late-orogenic evolution of Pyrenees and Liguro-Provençal rifting
Abstract The Pyrenean Belt ends against the Gulf of Lion passive margin. The mechanism
responsible for dismantling the mountain belt during Oligocene rifting has not yet found a …
responsible for dismantling the mountain belt during Oligocene rifting has not yet found a …